期刊文献+

秋季黄河口滨岸潮滩湿地系统CH_4通量特征及影响因素研究 被引量:5

Methane Fluxes and Controlling Factors in the Intertidal Zone of the Yellow River Estuary in Autumn
收藏 分享 导出
摘要 2009年秋季(9、10月),运用静态暗箱-气相色谱法对黄河口滨岸潮滩湿地系统的CH4排放通量进行了观测,并对影响CH4通量特征的关键因子进行了识别.结果表明,在空间上,秋季高潮滩、中潮滩、低潮滩和光滩的CH4通量范围分别为-0.206~1.264、-0.197~0.431、-0.125~0.659、-0.742~1.767 mg.(m2.h)-1,均值为0.089、0.038、0.197和0.169mg.(m2.h)-1,均表现为CH4排放源,但源功能整体表现为低潮滩〉光滩〉高潮滩〉中潮滩;在时间上,9、10月的CH4排放通量范围分别为-0.444~1.767、-0.742~1.264 mg.(m2.h)-1,均值为0.218、0.028 mg.(m2.h)-1,除9月高潮滩表现为CH4弱汇外,其它潮滩的CH4通量均明显高于10月.研究发现,黄河口滨岸潮滩湿地环境因素变化比较复杂,CH4排放通量受多重因素控制.不同潮滩湿地在9、10月CH4排放通量的差异可能主要与温度(特别是气温)以及植被生长状况的差异有关,而水盐条件和潮汐状况对潮滩湿地系统CH4通量特征的影响也不容忽视. The characteristics of methane(CH4) fluxes from tidal wetlands of the Yellow River estuary were observed in situ with static-chamber and GC methods in September and October 2009,and the key factors affecting CH4 fluxes were discussed.From the aspect of space,the CH4 flux ranges in high tidal wetland,middle tidal wetland,low tidal wetland,bare flat are-0.206-1.264,-0.197-0.431,-0.125-0.659 and-0.742-1.767 mg·(m2·h)-1,the day average fluxes are 0.089,0.038,0.197 and 0.169 mg·(m2·h)-1,respectively,indicating that the tidal wetlands are the sources of CH4 and the source function of CH4 differed among the four study sites,in the order of low tidal wetlandbare flathigh tidal wetlandmiddle tidal wetland.From the aspect of time,the ranges of CH4 fluxes from the tidal wetland ecosystems are-0.444-1.767 and-0.742-1.264 mg·(m2·h)-1,and the day average fluxes are 0.218 and 0.028 mg·(m2·h)-1 in September and October,respectively.The CH4 fluxes in each tidal wetland in September are higher than those in October except that the high tidal wetland acts as weak sink in September.Further studies indicate that the changes of environmental factors in the Yellow River estuary are complicated,and the CH4 fluxes are affected by multiple factors.The differences of CH4 fluxes characteristics among different tidal wetlands in autumn are probably related to temperature(especially atmospheric temperature) and vegetation growth status,while the effects of water or salinity condition and tide status on the CH4 flux characteristics might not be ignored.
作者 姜欢欢 孙志高 王玲玲 牟晓杰 孙万龙 宋红丽 孙文广 JIANG Huan-huan,SUN Zhi-gao,WANG Ling-ling,MOU Xiao-jie,SUN Wan-long,SONG Hong-li,SUN Wen-guang(1.Key Laboratory of Coastal Environment Processes,Shandong Provincial Key Laboratory of Coastal Zone Environmental Processes,Yantai Institute of Coastal Zone Research,Chinese Academy of Sciences,Yantai 264003,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China;3.Northeast Institute of Geography and Agroecology,Chinese Academy of Sciences,Changchun 130012,China)
出处 《环境科学》 CAS CSCD 北大核心 2012年第2期 565-573,共9页 Chinese Journal of Environmental Science
基金 国家自然科学基金项目(40803023 41171424) 国家海洋局海洋-大气化学与全球变化重点实验室基金项目(GCMAC1002) 中国科学院战略性先导科技专项(XDA05030404-2) 山东省自然科学基金重点项目(ZR2010DZ001) 中国科学院知识创新工程重要方向项目(KZCX2-YW-223)
关键词 潮滩湿地 甲烷 通量特征 影响因素 黄河口 秋季 tidal wetland methane flux characteristic controlling factor Yellow River estuary autumn
作者简介 姜欢欢(1986~),女,硕士研究生,主要研究方向为湿地生物地球化学,E-mail:hhjiang13@163.com 通讯联系人,E-mail:zgsun@yic.ac.cn
  • 相关文献

参考文献36

二级参考文献534

共引文献474

同被引文献164

引证文献5

二级引证文献10

投稿分析

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部 意见反馈